Zobrazeno 1 - 10
of 11
pro vyhledávání: '"William R. Dupre"'
Autor:
William R. Dupre, Mervin J. Bartholomew, Taylor F. Armstrong, William T. Jackson, Kevin G. Stewart
Publikováno v:
Journal of Sedimentary Research. 86:394-407
Paleoseismites, in the form of clastic dikes and sills and convolute bedding record syndepositional tectonism prior to lithification, fold growth, and onset of major orogenic events. The Elk Basin anticline, located in the northern portion of the Big
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8d9aabcdc75b8b1a934bef371d816030
https://doi.org/10.2110/jsr.2016.28
https://doi.org/10.2110/jsr.2016.28
Publikováno v:
Journal of Sedimentary Research. 85:445-458
Confluence scours in braided rivers occur where channel threads join together, producing erosional relief that may be considerably deeper than average channel depth. Based on studies of the continental-scale Ganges–Brahmaputra river system, it has
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b20af7cfdb88496db791f07397690f26
https://doi.org/10.2110/jsr.2015.34
https://doi.org/10.2110/jsr.2015.34
Publikováno v:
Geological Society of America Bulletin. 122:926-945
We investigated the interaction among basin-bounding faults, basin fi ll, and geomorphic features of the southern Gar Basin, one of only two known releasing double-bend basins along the Karakoram fault, to better understand their structural evolution
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2cb5e5200117d43ccc04557db63121c3
https://doi.org/10.1130/b26566.1
https://doi.org/10.1130/b26566.1
Autor:
W. R. Lettis, T. K. Rockwell, J. R. Unruh, A. M. Sarna-Wojcicki, C. L. Powell, S. A. Mathieson, R. B. Morrison, P. F. McDowell, H. E. Clifton, D. J. Ponti, William R. Dupre, R. S. Yeats, E. L. Leithold, K. R. Lajoie
Publikováno v:
Quaternary Nonglacial Geology: Conterminous U.S.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::13a49e57c59fabca26c87e6d8e3609fd
https://doi.org/10.1130/dnag-gna-k2.141
https://doi.org/10.1130/dnag-gna-k2.141
Autor:
William R. Dupre, Oluwayomi A. Oyedele
Publikováno v:
Day 3 Wed, May 07, 2014.
Abstract The study area is located within the Mad Dog Development Area in the Gulf of Mexico. Several studies have been carried out in the area including the use of coherence and seismic amplitudes to identify fan sands behind the prominent Sigsbee E
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cae71030a48ec4fa89dfee5582e363e9
https://doi.org/10.4043/25168-ms
https://doi.org/10.4043/25168-ms
Autor:
Ian Evans, William R. Dupre
Publikováno v:
Journal of Geoscience Education. 48:431-435
We have used a variety of approaches to introduce quantitative concepts into our introductory geology classes, some of which rely on using case studies of local rivers to improve student interest and appreciation of quantitative methods in scientific
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::55bf4fa709d57374aa718d33edba9471
https://doi.org/10.5408/1089-9995-48.4.431
https://doi.org/10.5408/1089-9995-48.4.431
Publikováno v:
Open-File Report.
This Open-File report is a digital geologic map database stored in a computer in the U. S. Geological Survey offices in Menlo Park, California. The study area includes the Monterey Peninsula and part of the Carmel Valley area. Geologically, this regi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4ee830432f82b0740c1aac3ce0134d73
https://doi.org/10.3133/ofr9730
https://doi.org/10.3133/ofr9730
Publikováno v:
Geosphere. 7:1209
The Silver City Range in southwest New Mexico contains Proterozoic basement rocks that are overlain by a sequence of Paleozoic, Mesozoic, and Paleogene strata. These rocks are folded in a broad, NW-SE–trending, east-facing monocline that lies struc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::14fdd47257db4559f9a21b29c9b5adcd
https://doi.org/10.1130/ges00672.1
https://doi.org/10.1130/ges00672.1
Autor:
William R. Dupre
The central Monterey Bay region (Figure 1) has been a stable to subsiding depocenter and the locus of fluvial, alluvialfan, and eollan activity throughout the Quaternary. It and adjacent tectonically uplifting areas provide an opportunity to study th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0ec2a687dc0bddadb220523e89a38895
https://doi.org/10.32375/1990-gb67.12
https://doi.org/10.32375/1990-gb67.12